ERC Starting Grant · 2018
Europe was the continent where Neanderthal and Anatomically Modern Human (AMH) interacted in a supposed time window of up to five millennia around 40,000 years ago (40 ka BP). The fate of our species versus the demise of Neanderthals, the geospatial timing of this process, the behavioural implications of their interaction, are hotly debated topics in archaeology. In this context, chronology plays a pivotal role, with radiocarbon (14C) dating representing the backbone back to 50 ka BP. However, due to varying atmospheric 14C concentrations in the past, the method requires calibration to an independently dated archive. So far, only the past 14 ka BP can profit from the most direct natural…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.